HIGHLIGHTS
SUMMARY
Future PWC change is tightly associated with the spatial pattern of tropical Pacific SST warming under the control of Bjerknes feedback (Zebiak and Cane 1987; Xie et_al 2010; Tokinaga et_al 2012; Wang et_al 2021). Besides the SST warming pattern, the land-sea thermal contrast, variations in the western north Pacific monsoon, 4 the Indonesian throughflow, and the Leeuwin current are associated with the response of the PWC to a warming climate (Feng et_al 2011; Zhang and Li 2016; Yim et_al The authors used CMIP6 outputs to analyze the PWC change in response to greenhouse . . .
If you want to have access to all the content you need to log in!
Thanks :)
If you don't have an account, you can create one here.